The North Branch of the Gale River is a 5.8-mile (9.3 km) long river in the White Mountains of New Hampshire in the United States. Via the Gale River, it is a tributary of the Ammonoosuc River and part of the Connecticut River watershed.
The North Branch rises in the valley between South Twin and Galehead mountains, just north of the AMC Galehead Hut. It flows northwest out of the mountains, largely followed by the Gale River Trail (a hiking trail), and joins the South Branch to form the Gale River at the crossing of U.S. Route 3. The North Branch provides drinking water to the town of Littleton, New Hampshire.
The Connecticut Lakes are a group of lakes in Coos County, northern New Hampshire, United States, situated along the headwaters of the Connecticut River. They are accessed via the northernmost segment of U.S. Route 3, between the village of Pittsburg and the Canada port of entry south of Chartierville, Quebec. The lakes are located within the boundaries of Pittsburg, but are far from the town center. Connecticut Lakes State Forest adjoins them.
There are four lakes: First, Second, Third and Fourth Connecticut Lake, numerically running south to north. The lakes decrease in size and increase in elevation, sequentially from first to fourth. The fourth lake is the source of the Connecticut River. The first three lakes can be viewed and accessed from U.S. Route 3, while the only access to the fourth lake is via the Fourth Connecticut Lake Trail, which goes in and out of Canada. All lakes are north of the 45th parallel.
Lake Francis lies to the south of the four Connecticut Lakes. It is a man-made reservoir and the last of the major lakes along the Connecticut River in northern New Hampshire.Dublin Pond
Dublin Pond or Dublin Lake is a 236-acre (0.96 km2) water body located in Cheshire County in southwestern New Hampshire, United States, in the town of Dublin. The pond lies at an elevation of 1,480 feet (451 m) above sea level, near the height of land between the Connecticut River/Long Island Sound watershed to the west and the Merrimack River/Gulf of Maine watershed to the east.Gale River
The Gale River is a 13.1-mile (21.1 km) long tributary of the Ammonoosuc River in northwestern New Hampshire in the United States. Via the Ammonoosuc, it is part of the watershed of the Connecticut River, which flows to Long Island Sound.
The Gale River flows for its entire length in Grafton County. It rises in the White Mountains in the town of Franconia as two short, northward-flowing streams: its North Branch and its South Branch. The two streams join in Bethlehem, and the Gale River flows thence generally westwardly. Returning to Franconia, the river collects the Ham Branch, its most significant tributary, then passes through Sugar Hill to Lisbon, where it joins the Ammonoosuc River.Lake Francis (Murphy Dam)
Lake Francis is a reservoir on the Connecticut River in northern New Hampshire, United States. The lake is located in Coos County, east of the village of Pittsburg and along the boundary between the towns of Pittsburg and Clarksville. The lake is impounded by Murphy Dam, built in 1940 as a flood control project. The 117-foot (36 m) earthen dam is owned by the Water Division of the state's Department of Environmental Services, and is operated by TC Energy (formerly TransCanada Corporation).Lake Francis and Murphy Dam are named after Francis P. Murphy, who served as the Governor of New Hampshire from 1937 to 1941. The lake covers nearly 2,000 acres (8 km2), has a capacity of 131,375 acre feet (162,049,000 m3), and has average and maximum depths of 40 feet (12 m) and 82 feet (25 m), respectively.The lake is classified as a coldwater fishery, with observed species including rainbow trout, brown trout, landlocked salmon, lake trout, and chain pickerel. There are two public boat launch locations, and ice fishing is permitted from January through March.Lake Francis State Park is located on the northeast side of the lake, where the Connecticut River flows in. North of Lake Francis is Back Lake, while First Connecticut Lake (one of a series of four Connecticut Lakes that serve as the headwaters of the Connecticut River) lies to the northeast.List of rivers of New Hampshire
This is a list of rivers and significant streams in the U.S. state of New Hampshire.
All watercourses named "River" (freshwater or tidal) are listed here, as well as other streams which are either subject to the New Hampshire Comprehensive Shoreland Protection Act or are more than 10 miles (16 km) long. New Hampshire rivers and streams qualify for state shoreland protection (and are listed here in bold) if they are fourth-order or larger water bodies, based on the Strahler method of stream order classification.Saville Dam
Saville Dam is an earthen embankment dam with masonry work on the eastern branch of the Farmington River in southwestern Barkhamsted, Connecticut. The dam is 135 ft. (41 m) tall and 1,950 ft. (590 m) long and has an uncontrolled spillway on its western portion. It creates the Barkhamsted Reservoir which has a volume of 36.8 billion US gallons (139,000,000 m3) and is the primary water source for Hartford, Connecticut.
In 1927, the Metropolitan District Commission began to purchase land in the present-day footprint of the dam and reservoir. Construction of the dam commenced in 1936 while land to the north was being stripped of lumber and buildings.
Before the Metropolitan District Commission named the Saville Dam in 1940 in honor of its chief engineer, Caleb Mills Saville, it was referred to as the Bill's Brook Dam after the brook that ran near the site at the time.
The foundations for "Bill's Brook Dam" and the diversion tunnel for the East Branch of the Farmington River were completed in August 1934. Subsequently, the East Branch was diverted into the concrete conduit at the bottom of the Bill's Brook Dam site. The dam was completed in May 1940, at a total cost for dam and reservoir of $10M.Although the Saville Dam was completed in 1940, it was not until 1948 that the Barkhamsted Reservoir finally filled to capacity. The Farmington River East Branch is impounded for nearly 8 miles (13 km) behind the dam, with the northernmost open waters of Barkhamsted Reservoir terminating in Hartland, Connecticut just south of the Massachusetts border.The reservoir flooded many buildings and farms of Barkhamsted, including the village of Barkhamsted Hollow. The village of Barkhamsted Center, partially flooded, lies just to the west of the reservoir. Its remaining buildings are part of the Barkhamsted Center Historic District, listed on the National Register of Historic Places.
|Gulf of Maine|
|Long Island Sound|